The mistery of Jupiter jets begins to unveil

Comunicado de prensa en español

An international team leaded by researchers from the Universidad del País Vasco studys the interaction of two giant storms in Jupiter with the strongest jet of the planet

This work is the cover in the Nature review on 24 January 2008.




Press release from:
MEDIA RELATIONS OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109 TELEPHONE 818-354-5011
http://www.jpl.nasa.gov

Carolina Martinez 818-354-9382
Jet Propulsion Laboratory, Pasadena, Calif.


GIANT STORM ERUPTION AT JUPITER UNEARTHS A BURIED PAST

At the end of March 2007, scientists around the globe observed an astonishing and rare change in Jupiter's atmosphere-a huge disturbance churning in the middle northern latitudes of the giant planet as two giant storms erupted.

Jupiter's winds are the strongest at middle northern latitudes, reaching about 600 kilometers per hour (370 miles). Similar phenomena occurred in 1975 and 1990, but this event has never been observed before with the high resolution of modern telescopes.

An international team coordinated by Agustín Sánchez-Lavega from the Universidad del País Vasco in Spain presents their findings about this event in the January 24 issue of the journal Nature.

The team monitored the new eruption of cloud activity and its evolution with an unprecedented resolution using NASA'S Hubble Space Telescope, the NASA Infrared Telescope Facility in Hawaii and telescopes in the Canary Islands (Spain). A network of smaller telescopes around the world also supported these observations.

"Fortuitously, we captured the onset of the disturbance with Hubble, while monitoring the planet to support the New Horizons flyby observations of Jupiter in its route to Pluto. We saw the rapidly growing storm since its beginning from about 400 kilometers (250 miles) to more than 2,000 kilometers (1,245 miles) in size in less than one day," indicates Sánchez-Lavega.

According to the analysis, the bright plumes were storm systems triggered in Jupiter's deep water clouds that moved upward in the atmosphere vigorously and injected a fresh mixture of ammonia ice and water about 30 kilometers (20 miles) above the visible clouds. The storms moved in the peak of a jet stream in Jupiter's atmosphere at 600 kilometers per hour (375 miles per hour). The storms disturbed the jet and formed in their wake a turbulent planetary-scale disturbance containing red aerosols.

"The infrared images distinguish the plumes from lower-altitude clouds and show that the plumes are lofting ice particles higher than anyplace else on the planet," said Glenn Orton, from NASA's Jet Propulsion Laboratory, Pasadena, Calif., and second author of the paper.

In spite of the energy deposited and the stirring and turmoil generated by the storms, the jet remained practically unchanged when the disturbance ceased, keeping steady against these storms. Models of the disturbance indicate that the jet stream extends deep in the buried atmosphere of Jupiter, more than 100 kilometers (62 miles) below the cloud tops where most sunlight is absorbed.

"This confirms previous findings by the Galileo Probe when it descended through Jupiter's upper atmosphere in December 1995. Although both regions are meteorologically different, all the evidence points to a deep extent for Jupiter's jets and suggest that the internal heat power source plays a significant role in generating the jet," indicates Sánchez-Lavega.

A comparison of this disturbance with the two previous events in 1975 and 1990 shows surprising similarities and coincidence, all of which remain unexplained. All three eruptions occurred with a periodic interval of about 15 to 17 years. The plumes always appear in the jet peak; the disturbance erupted with exactly two plumes (no more and no less). Finally, the plumes moved with the same speed of the jet peak in all three events. Understanding this outbreak could be the key to unlock the mysteries buried in the deep Jovian atmosphere.

The atmosphere of the gaseous giant planet Jupiter, 10 times the size of Earth, is always turbulent. Its circulation is dominated by a pattern of cloud bands alternating with latitude and by a persistent system of jet streams, both of unknown origin. Changes in the cloud bands are sometimes violent, starting from a localized eruption and followed by the development of a planetary scale disturbance. The nature of these disturbances and the power source for these jets remains a controversial matter among planetary scientists and meteorologists. They could be powered by the sun as is Earth, by the strong internal heat source emanating from Jupiter's interior, or by a combination of both.

Understanding these phenomena is important for Earth's meteorology where storms are present everywhere and jet streams dominate the atmospheric circulation. In this way, Jupiter represents a natural laboratory where atmospheric scientists study the nature and interplay of the intense jets and severe atmospheric phenomena.


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Additional pictures and material:


The history of a North Temperate Belt Disturbance. The history of the North Temperate Belt of Jupiter just before the onset of the perturbations (left), during the turbulent intermediate stage (center) and after the perturbations dissipated (right). Note the change in colour in the left and right images. All pictures acquired by the Hubble Space Telescope.


Merging the infrared view of Jupiter's upper atmosphere and the view from Hubble Space Telescope. The infrared image on the left (NASA-IRTF) shows the heads of both convective plumes high in the atmosphere. The right image (HST) shows the turbulence formed as a consecuence on the latitude range of Jupiter's North Temperate Belt.


Nearly simultaneous view of the storms and jet in the infrared (left, NASA-IRTF) and in the visible (right, Zac Pujic). The storms are particularly bright in a wavelength of 2.3 microns representative of very high levels in the atmosphere. The visible image shows the pattern of turbulence formed on the wake of the plumes.